Neptunium ( , ) is a
chemical element with the symbol
Np and
atomic number
93. A
radioactive metallic element,
neptunium is the first
transuranic
element and belongs to the
actinide
series. Its most stable
isotope,
237Np, is a by-product of
nuclear reactors and
plutonium production and it can be used as a
component in
neutron detection
equipment. Neptunium is also found in trace amounts in
uranium ores due to transmutation reactions.
Characteristics
Silvery in appearance, neptunium
metal is
fairly chemically
reactive and is
found in at least three
allotropes:
- α-neptunium, orthorhombic, density
20.45 g/cm³
- β-neptunium (above 280 °C), tetragonal, density (313 °C) 19.36 g/cm³
- γ-neptunium (above 577 °C), cubic, density (600 °C) 18
g/cm³
Compounds
This element has four ionic
oxidation
states while in solution:
- Np3+ (pale purple), analogous to the rare earth ion
Pm3+
- Np4+ (yellow green)
- NpO2+ (green blue)
- NpO22+ (pale pink)
Neptunium forms tri- and tetra
halides such as
NpF
3, NpF
4, NpCl
4,
NpBr
3, NpI
3, and
oxides
of the various compositions such as are found in the
uranium-
oxygen system, including
Np
3O
8 and NpO
2.
Neptunium(V) fluoride, NpF
5, is volatile like
uranium hexafluoride.
Neptunium, like other actinides, readily forms a dioxide neptunyl
core (NpO
2), which readily complexes with carbonate as
well as other oxygen moieties (OH
−,
NO
2−, NO
3−, and
SO
42−) to form charged complexes which tend
to be readily mobile with low affinities to soil.
- NpO2(OH)2−
- NpO2(CO3)−
- NpO2(CO3)23−
- NpO2(CO3)35−
Uses
Precursor in Plutonium-238 Production
237Np is irradiated with neutrons to create
238Pu, an
alpha emitter for
radioisotope thermal
generators for spacecraft and military applications.
237Np will capture a neutron to form
238Np
and beta decay with a half life of two days to
238Pu.
- \mathrm{^{237}_{\ 93}Np\ +\ ^{1}_{0}n\ \longrightarrow \
^{238}_{\ 93}Np\ \xrightarrow[2.117 \ d]{\beta^-} \ ^{238}_{\
94}Pu}
238Pu also exists in sizable quantities in
spent nuclear fuel but would have to be
separated from other
isotopes of
plutonium.
Weapons applications
Neptunium is
fissionable, and could
theoretically be used as fuel in a
fast neutron reactor or a
nuclear weapon. In 1992, the
U.S. Department of Energy declassified
the statement that Np-237 "can be used for a nuclear explosive
device". It is not believed that an actual weapon has ever been
constructed using neptunium. Calculations show that the critical
mass is between 50 and 60 kg. As of 2009, the world production
of Np-237 by commercial power reactors was over 1000 critical
masses a year, but to extract the isotope from irradiated fuel
elements would be a major industrial undertaking.
In
September 2002, researchers at the University of California Los Alamos
National Laboratory
created the first known nuclear critical mass using neptunium in combination
with enriched uranium, discovering
that the critical mass of neptunium is around 60 kg, showing
that it "is about as good a bomb material as U-235." US officials in March 2004,
planned to move the nation's supply of separated neptunium to a
site in Nevada.
Other
237Np is used in devices detecting high-energy (MeV)
neutrons.
History
At least three times discoveries of the element 93 were falsely
reported, namely as
Bohemium on one hand
and
Ausonium one another in 1934 and then
as
Sequanium in 1939.
Neptunium (named for the planet
Neptune, the
next
planet out from
Uranus, after which
uranium
was named) was first
discovered by
Edwin McMillan and
Philip H. Abelson in the year 1940 in Berkeley,
California.
Initially predicted by Walter Russell's "spiral" organization of the
periodic table, it was found at the Berkeley Radiation Laboratory
of the University of California,
Berkeley
where the team produced the neptunium isotope 239Np (2.4 day half-life) by bombarding uranium with slow moving neutrons. It was the
first
transuranium element
produced synthetically and the first
actinide series transuranium element
discovered.
- \mathrm{^{238}_{\ 92}U\ +\ ^{1}_{0}n\ \longrightarrow \
^{239}_{\ 92}U\ \xrightarrow[23 \ min]{\beta^-} \ ^{239}_{\ 93}Np\
\xrightarrow[2.355 \ d]{\beta^-} \ ^{239}_{\ 94}Pu}
Occurrence
Trace amounts of neptunium are found naturally as
decay products from
transmutation reactions in
uranium ores. Artificial
237Np is
produced through the
reduction of
237NpF
3 with
barium or
lithium vapor at around 1200 °
C and is most often extracted from spent
nuclear fuel rods as a by-product in
plutonium production.
- 2 + 3 Ba → 2 Np + 3
By weight, neptunium-237 discharges are about 5 % as great as
plutonium discharges and about 0.05 % of
spent nuclear fuel discharges.
Synthesis
Chemically, neptunium is prepared by the reduction of
NpF
3 with barium or lithium vapor at about 1200 °C,
however, most Np is produced in nuclear reactions:
- When an 235U atom
captures a neutron, it is converted to an excited state of 236U. About 81 % of the excited
236U nuclei undergo fission, but the remainder decay to
the ground state of 236U by emitting gamma radiation. Further neutron capture creates 237U
which has a half-life of 7 days and thus quickly decays to
237Np.
- :\mathrm{^{235}_{\ 92}U\ +\ ^{1}_{0}n\ \longrightarrow \
^{236}_{\ 92}U_m\ \xrightarrow[120 \ ns]{} \ ^{236}_{\ 92}U\ +\
\gamma}
- :\mathrm{^{236}_{\ 92}U\ +\ ^{1}_{0}n\ \longrightarrow \
^{237}_{\ 92}U\ \xrightarrow[6.75 \ d]{\beta^-} \ ^{237}_{\
93}Np}
- 237U is also produced via an (n,2n) reaction with 238U. This only happens with very
energetic neutrons.
- 237Np is the product of alpha
decay of 241Am.
Heavier isotopes of neptunium decay quickly, and lighter isotopes
of neptunium cannot be produced by
neutron capture, so chemical separation of
neptunium from cooled
spent nuclear
fuel gives nearly pure
237Np.
Role in nuclear waste
Neptunium-237 is the most mobile
actinide
in the
deep geological
repository environment.This makes it and its predecessors such
as
americium-241 candidates of
interest for destruction by
nuclear transmutation. Neptunium
accumulates in commercial household ionization-chamber smoke
detectors from decay of the (typically) 0.2
microgram of americium-241 initially present as a
source of
ionizing radiation.
With a half-life of 432 years, the americium-241 in a smoke
detector includes about 5 % neptunium after 22 years, and about 10
% after 43 years. After the 432-year americium-241 half-life, a
smoke detector's original americium would be almost half
neptunium.
Due to its long half life neptunium becomes the major contributor
of the total radiation in 10000 years. As it is unclear what
happens to the containment in that long time span, an extraction of
the neptunium would minimize the contamination of the environment
if the nuclear waste could be mobilized after several thousand
years.
Isotopes
19 neptunium
radioisotopes have been
characterized, with the most stable being
237Np with a
half-life of 2.14 million years,
236Np with a half-life of 154,000 years, and
235Np with a half-life of 396.1 days. All of the
remaining
radioactive isotopes have
half-lives that are less than 4.5 days, and the majority of these
have half-lives that are less than 50 minutes. This element also
has 4
meta states, with the most stable
being
236mNp (t
½ 22.5 hours).
The isotopes of neptunium range in
atomic
weight from 225.0339
u
(
225Np) to 244.068 u (
244Np). The primary
decay mode before the most stable
isotope,
237Np, is
electron
capture (with a good deal of
alpha
emission), and the primary mode after is
beta emission. The primary
decay products before
237Np are
element 92 (
uranium) isotopes (alpha
emission produces element 91,
protactinium, however) and the primary products
after are element 94 (
plutonium)
isotopes.
237Np is
fissionable.
237Np eventually decays to form
bismuth-209, unlike most other common heavy nuclei
which decay to make
isotopes of
lead. This
decay chain is known as
the
neptunium series.
References
- "Restricted Data Declassification Decisions from
1946 until Present", accessed Sept 23, 2006
Literature
- Guide to the Elements - Revised Edition, Albert
Stwertka, (Oxford University Press; 1998) ISBN 0-19-508083-1
- Lester R. Morss, Norman M. Edelstein, Jean Fuger (Hrsg.):
The Chemistry of the Actinide and Transactinide Elements,
Springer-Verlag, Dordrecht 2006, ISBN 1-4020-3555-1.
- Ida Noddack: "Über das Element 93",
in: Angewandte Chemie
1934, 47, 653–655.
External links